Preprints
https://doi.org/10.5194/egusphere-2026-3837
https://doi.org/10.5194/egusphere-2026-3837
30 Jul 2026
 | 30 Jul 2026
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Enhanced production and methylation of bacterial branched tetraether lipids responding to water content-mediated redox changes in Tibetan Plateau permafrost soils

Wan Zhang, Xiaotong Tang, Wenyong Yao, Jing Qian, Wei He, Yanhong Zheng, Yuanqing Zhu, Ronnakrit Rattanasriampaipong, Yufei Chen, Fengfeng Zheng, and Chuanlun Zhang

Abstract. Branched glycerol dialkyl glycerol tetraethers (branched GDGTs) are bacterial membrane lipids widely used as biomarkers for terrestrial and marine paleoenvironmental reconstruction. Sparsely branched and overly branched GDGTs (sb- and ob-GDGTs) are predominantly detected in anaerobic environments and have been proposed as redox proxies in marine settings. However, their distributions, environmental controls, and biological sources in terrestrial environments remain poorly understood. Here, we investigated the distributions of sb/br/ob-GDGTs, together with bacterial community composition in two permafrost peatland soil profiles from the Tibetan Plateau. Our results demonstrate that elevated soil water content (SWC) influences branched GDGT composition by creating anaerobic conditions that promote the production and methylation of sb/br/ob-GDGTs. Co-occurrence network analyses revealed strong positive correlations between the relative abundances of sb/br/ob-GDGTs and anaerobic bacterial communities, including taxa affiliated with Proteobacteria, Caldithrix, Nitrospirae, Spirochaetes and Chloroflexi. These findings suggest that oxygen-limited conditions may reshape sb/br/ob-GDGT-producing bacterial communities in permafrost soils, thereby promoting the accumulation of sb/br/ob-GDGTs. Furthermore, we demonstrate that the methylation index of ob- and br-GDGTs (MIob/br) serves as a sensitive indicator for soil redox dynamics and may be applied to reconstruct paleohydrological variability, thereby aiding assessments of permafrost carbon-cycle feedbacks to climate warming.

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Wan Zhang, Xiaotong Tang, Wenyong Yao, Jing Qian, Wei He, Yanhong Zheng, Yuanqing Zhu, Ronnakrit Rattanasriampaipong, Yufei Chen, Fengfeng Zheng, and Chuanlun Zhang

Status: open (until 10 Sep 2026)

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Wan Zhang, Xiaotong Tang, Wenyong Yao, Jing Qian, Wei He, Yanhong Zheng, Yuanqing Zhu, Ronnakrit Rattanasriampaipong, Yufei Chen, Fengfeng Zheng, and Chuanlun Zhang
Wan Zhang, Xiaotong Tang, Wenyong Yao, Jing Qian, Wei He, Yanhong Zheng, Yuanqing Zhu, Ronnakrit Rattanasriampaipong, Yufei Chen, Fengfeng Zheng, and Chuanlun Zhang

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Short summary
Tibetan Plateau peatlands store large amounts of carbon and are sensitive to warming and changing water conditions. We studied two peatland profiles and found that soil water content can change the living conditions for microbes and alter the structures and amounts in their cell membranes. This response provides a useful signal for tracking past soil moisture and environmental change in cold mountain regions.
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